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Global compilation of benthic data sets I
Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary... -
Total organic carbon content in surface sediments, a compilation from differe...
This dataset has no description
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Environmental analysis of surface sediments from the Northwest African upwell...
This dataset has no description
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Abundance of organic-walled dinoflagellate cysts in surface sediments from th...
This dataset has no description
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Carbon and nitrogen data of surface sediment cores in the Canary Islands region
This dataset has no description
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Geochemistry of surface sediment cores in the Canary Islands region
This dataset has no description
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(Table S1) Diatom abundance in coastal upwelling systems
Coastal upwelling systems account for approximately half of global ocean primary production and contribute disproportionately to biologically driven carbon sequestration.... -
Grain-size analysis of surface sediments, continental margin off NW Africa
The terrigenous fraction of seabed sediments recovered along the north-west African continental margin illustrates spatial variability in grain size attributed to different... -
Organic-walled dinoflagellate cysts and environmental analysis of surface sed...
In order to examine the spatial distribution of organic-walled dinoflagellate cysts (dinocysts) in recent sediments related to environmental conditions in the water column,... -
Nutrients measured on water bottle samples at station VH96/1-3_049
771 days since 01.01.1994 -
Nutrients measured on water bottle samples at station VH96/1-3_031
765 days since 01.01.1994 -
Planktic foraminifera analyses of surface sediments and satellite data in the...
The Canary Islands region occupies a key position with respect to biogeochemical cycles, with the zonal transition from oligotrophic to nutrient-rich waters and the contribution... -
Planktic foraminifera in surface sediments
see satellite data doi:10.1594/PANGAEA.57967
